Perhaps first of all I wished to visit the South Pole—not an unreasonable1 ambition it would seem for one backed by ten generations of sea captains and ocean faring—but one that I found not altogether easy to gratify. For one thing, there was no Antarctic expedition forming at the time; and then, my notions in the matter were not popular.
From boyhood it had been my dream that about the earth’s southern axis2, shut in by a precipitous wall of ice, there lay a great undiscovered world. Not a bleak3 desolation of storm-swept peaks and glaciers4, but a fair, fruitful land, warmed and nourished from beneath by the great central heat brought nearer to the surface there through terrestrial oblation5, or, as my geography had put it, the “flattening of the poles.”
I had held to this fancy for a long time on the basis of theory only, and, perhaps, the added premise6 that nature would not allow so vast a tract7 as the Antarctic Continent to lie desolate8. But, curiously9 8enough, about the time I arrived in New York I met with what seemed to me undoubted bits of evidence in the reports of some recent polar observations.
Borchgrevink, a Norwegian explorer, returning with a poorly fitted Antarctic expedition, reported, among other things, a warm current off Victoria Land, at a point below the 71st parallel, and flowing approximately from the direction of the pole![1]
1. “It seems to me,” he says, in an article printed in the Century Magazine (January, 1896), “that an investigation10 of the origin and consequences of the warm current running northeast, which we experienced in Victoria Bay, is of the greatest importance.”
True, Borchgrevink believed the Antarctic Continent to be an exceptionally cold one, but for this he was not to blame. No man can help what he does or does not believe in these matters regardless of sound logic11 and able reasoning to the contrary.—N. C.
Nansen, another Norwegian, in the Arctic Polar Sea, had been astonished to find that the water at a great depth, instead of being colder than at the surface as he had expected, was warmer! He had also found that as he progressed northward12 from 80° the thermometer had been inclined to rise rather than to fall. To be sure, when he arrived at a point within a little more than two hundred miles of the earth’s axis, he had found only a continuance of ice—a frozen sea which undoubtedly13 extended to 9the pole itself; but this frigidity14 I attributed to the fact that it was a sea into which, from the zone of fierce cold below, were constantly forced huge ice-floes. These, as I conceived, would maintain the condition of cold in the Arctics by shutting out the under warmth, through which, however, they would be gradually melted—to be discharged in those great Arctic currents which Nansen and other explorers had observed. The lack of thickness in the ice forming about the pole had also been noted15 with some surprise. This too, I claimed, was due to the warm earth beneath it which, while it could not much affect the general climate, when some three miles of very chilly16 water and several feet of substantial ice lay between, did serve as a provision of nature to prevent the northern sea from becoming one mighty17 solidified18 mass.
Now, ice-floes could not be forced inland, as would have to be the case in the Antarctics where there was admittedly a continent instead of a sea. Around this continent, it was said, there lay a precipitous frozen wall which no man had ever scaled. What lay beyond, no man of our world had ever seen. But in my fancy I saw those ramparts of eternal ice receding19 inward to a pleasant land, as the snow-capped Sierras slope to the verdant20 plains of California. A pleasant land—a fair circular world—temperate in its outer zone, becoming even 10tropic at the center, and extending no less than a thousand miles from rim21 to rim. There, I believed, unknown to the world without, a great and perhaps enlightened race lived and toiled—loved and died.
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1
unreasonable
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adj.不讲道理的,不合情理的,过度的 | |
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2
axis
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n.轴,轴线,中心线;坐标轴,基准线 | |
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3
bleak
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adj.(天气)阴冷的;凄凉的;暗淡的 | |
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4
glaciers
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冰河,冰川( glacier的名词复数 ) | |
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5
oblation
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n.圣餐式;祭品 | |
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6
premise
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n.前提;v.提论,预述 | |
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7
tract
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n.传单,小册子,大片(土地或森林) | |
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8
desolate
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adj.荒凉的,荒芜的;孤独的,凄凉的;v.使荒芜,使孤寂 | |
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9
curiously
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adv.有求知欲地;好问地;奇特地 | |
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10
investigation
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n.调查,调查研究 | |
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11
logic
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n.逻辑(学);逻辑性 | |
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12
northward
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adv.向北;n.北方的地区 | |
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13
undoubtedly
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adv.确实地,无疑地 | |
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14
frigidity
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n.寒冷;冷淡;索然无味;(尤指妇女的)性感缺失 | |
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15
noted
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adj.著名的,知名的 | |
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16
chilly
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adj.凉快的,寒冷的 | |
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17
mighty
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adj.强有力的;巨大的 | |
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18
solidified
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(使)成为固体,(使)变硬,(使)变得坚固( solidify的过去式和过去分词 ); 使团结一致; 充实,巩固; 具体化 | |
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19
receding
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v.逐渐远离( recede的现在分词 );向后倾斜;自原处后退或避开别人的注视;尤指问题 | |
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20
verdant
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adj.翠绿的,青翠的,生疏的,不老练的 | |
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21
rim
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n.(圆物的)边,轮缘;边界 | |
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